簽到天數: 3291 天 [LV.Master]伴壇終老
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t02436|2014-3-7 11:37
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THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 12.6S
153.1E IS NOW LOCATED NEAR 14.3S 150.6E, APPROXIMATELY 125 NM NORTH-
NORTHEAST OF WILLIS ISLAND, AUSTRALIA. ANIMATED MULTISPECTRAL
SATELLITE IMAGERY DEPICTS A BROAD LOW-LEVEL CIRCULATION CENTER
(LLCC) WITH FORMATIVE CONVECTIVE BANDING WRAPPING INTO THE LLCC. A
062353Z METOP-B IMAGE SHOWS DEEP CONVECTIVE BANDING PERSISTING ALONG
THE SOUTHERN AND WESTERN FLANK OF THE BROAD LLCC. A 062353Z ASCAT
IMAGE SHOWS THE BROAD CIRCULATION CENTER BUT PROVIDES EVIDENCE THAT
THE SYSTEM IS SLOWLY STRENGTHENING WITH 25 TO 30 KNOT WINDS WRAPPING
INTO THE NORTHERN SEMI-CIRCLE. SURFACE OBSERVATIONS FROM WILLIS
ISLAND INDICATE 25 TO 30 KNOT SUSTAINED SOUTHEASTERLY WINDS. UPPER-
LEVEL ANALYSIS REVEALS AN IMPROVING ENVIRONMENT WITH LIGHT TO
MODERATE VERTICAL WIND SHEAR (10 TO 20 KNOTS) AND FAVORABLE OUTFLOW,
ESPECIALLY POLEWARD OUTFLOW, WHICH IS ENHANCED BY STRONG WESTERLIES
OVER CENTRAL AUSTRALIA. DYNAMIC MODELS CONTINUE TO TRACK THE SYSTEM
SOUTHWESTWARD WITH A SLOW INTENSIFICATION TREND. MAXIMUM SUSTAINED
SURFACE WINDS ARE ESTIMATED AT 25 TO 30 KNOTS. MINIMUM SEA LEVEL
PRESSURE IS ESTIMATED TO BE NEAR 1002 MB. DUE TO IMPROVED
ORGANIZATION AND FAVORABLE CONDITIONS, THE POTENTIAL FOR THE
DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS HIGH.
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